Cowlesite

A zeolite mineral which typically occurs as small white or colourless spheres in basalt.

Often occurs with other zeolite minerals.

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Information about Cowlesite

Cowlesite is a rare calcium aluminium silicate zeolite – an unusual member of the zeolite family in that it lacks a confirmed three-dimensional framework structure of the kind that defines most zeolites, and for a long time its structure was incompletely determined.

It forms as delicate, colourless to white orthorhombic platy to acicular crystals, typically very small, in the cavities of basaltic and other mafic volcanic rocks where it grows alongside other zeolites such as phillipsite, chabazite, and thomsonite.

Like all zeolites it is a hydrated aluminosilicate capable of reversible water loss, and its open porous structure can host and exchange cations – the property that makes zeolites industrially important.

Cowlesite is one of the less commonly encountered zeolite species in collections, partly because of its very small crystal size and partly because it lacks the striking habit of some other zeolites. Careful examination of basalt vugs, however, sometimes reveals it as a component of the diverse zeolite assemblages that form by low-temperature hydrothermal alteration of basaltic glass in oceanic island and flood basalt sequences.

 


Uses and History

Cowlesite was named in honour of John Cowles, an American mineral collector who contributed specimens and enthusiasm to its discovery.

It occurs in the zeolite-bearing basalts of Oregon and Washington, USA; in Iceland, which has exceptionally rich zeolite-bearing volcanic sequences; and in various other basaltic provinces worldwide.

Cowlesite is not a significant British mineral in a collecting context, though zeolite-bearing basalts occur in parts of Scotland and Northern Ireland (particularly the Antrim basalts of the British Tertiary Igneous Province) that have the appropriate lithology and hydrothermal history.

 


Mineralogy

Chemistry
A hydrated calcium aluminium silicate zeolite, formula CaAl2Si3O106H2O. Unusual among zeolites in having an incompletely determined framework topology.
Colours and Variations
Colourless to white
Streak
White
Lustre
Vitreous to silky
Transparency
Transparent to translucent
Fracture
Irregular; good cleavage on {010}
Tenacity
Brittle
Crystal habit
Small platy to acicular orthorhombic crystals; aggregates in vesicle fillings in basalt
Crystal system
Orthorhombic
Mohs hardness
5.0-5.5
Fluorescence
Non-fluorescent
Specific Gravity
2.06-2.14
Easiest testing method
Colourless to white platy or acicular crystals in basalt cavities in company with other zeolites are suggestive of cowlesite, but definitive identification from other colourless zeolites (thomsonite, phillipsite, etc.) requires X-ray diffraction. Zeolites in general can be identified as a group by their low specific gravity, vitreous to silky lustre, and occurrence in basaltic vesicle fillings.

Hazards and Warnings

No specific hazards are associated with cowlesite under normal handling conditions. Standard precautions apply when cutting.

Almost all rocks, minerals (and, frankly, almost all other substances on earth) can produce toxic dust when cutting, which can cause serious respiratory conditions including silicosis. When cutting or polishing rocks, minerals, shells, etc, all work should be done wet to minimise the dust, and a suitable respirator or extraction system should be used.

 


Translations

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  • Cowlesite

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  • Cowlésite

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  • Cowlesita

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Further Reading / External Links